
sedimentary
Chert (Yellow Jasper variant)
Microcrystalline Quartz (SiO2)
Hardness: 6.5–7 on Mohs scale; Color: Honey-yellow to ochre (caused by iron oxide inclusions); Luster: Waxy to dull; Crystal structure: Cryptocrystalline; Cleavage: None (conchoidal fracture); Specific gravity: 2.65.
- Hardness
- 6
- Color
- Honey-yellow to ochre (caused by iron oxide inclusions)
- Luster
- Waxy to dull
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Physical properties
Hardness: 6.5–7 on Mohs scale; Color: Honey-yellow to ochre (caused by iron oxide inclusions); Luster: Waxy to dull; Crystal structure: Cryptocrystalline; Cleavage: None (conchoidal fracture); Specific gravity: 2.65.
Formation & geological history
Formed through the accumulation of silica-rich organic remains (like radiolarians or diatoms) or by chemical precipitation from groundwaters in limestone or shale beds. Common in stratigraphic layers from the Paleozoic to Mesozoic eras.
Uses & applications
Historically used for stone tools (arrowheads, scrapers) due to its sharp conchoidal edges; currently used in jewelry (decorative cabochons), landscape gravel, and as a component in concrete.
Geological facts
Yellow chert/jasper was prized by Neolithic peoples for tool-making; it can create sparks when struck against steel, making it useful for fire-starting in survival situations.
Field identification & locations
Identify in the field by its smooth, waxy surface and shell-like (conchoidal) fracture lines. It is common in riverbeds and limestone outcrops globally. Tips for collectors: check for translucency at thin edges to distinguish from similar opaque rocks.
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